cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.6084/m9.figshare.26656645.v1
title: Additional file 12 of Integrative transcriptomics reveals association of abscisic acid and lignin pathways with cassava whitefly resistance

description: Additional file 12: Table S24. Numbers of up- and down-regulated tDEGs in Arabidopsis during hormone treatments
DOI: 10.6084/m9.figshare.26656645
title: Additional file 12 of Integrative transcriptomics reveals association of abscisic acid and lignin pathways with cassava whitefly resistance

description: Additional file 12: Table S24. Numbers of up- and down-regulated tDEGs in Arabidopsis during hormone treatments
DOI: 10.1594/pangaea.777542
title: (Table 4) Age marks in bottom sediments from DSDP Leg 6 holes, Pacific Ocean
DOI: 10.1594/pangaea.815154
title: (Table 5b) Results of Rb-Sr measurements in Upper Vendian clayey rocks of the Russian Platform from the borehole Nevel_1-R
DOI: 10.1594/pangaea.770366
title: (Table 1) Lead isotope ratios of zircons from sample 122 of ODP Hole 153-922A

description: According to the theory of plate tectonics, rocks found in the vicinity of mid-ocean ridges - where oceanic plates are created - should be relatively young (at most several Myr old). Here we report the discovery of zircons with ages of about 330 and 1,600 Myr that were drilled from exposed gabbros beneath the Mid-Atlantic Ridge near the Kane fracture zone (Cannat and ODP Shipboard Scientific Party, 1995; Werner, 1997, doi:10.2973/odp.proc.sr.153.031.1997; Werner and Pilot, 1997, doi:10.2973/odp.proc.sr.153.018.1997; Pilot et al., 1996). Age determinations were made using the 207Pb/206Pb evaporation method (Kober, 1987, doi:10.1007/BF00375526) and confirmed with conventional U–Pb dating and ion microprobe (SHRIMP) analysis. We suggest two plausible explanations for the origin of these unusually old zircons. During the opening of the Atlantic, sheared crustal material or delaminated continental lithosphere sank into small roll-like circulation cells (Nocolas, 1995; Rabinowicz et al., 1984, doi:10.1016/0012-821X(84)90042-6) that developed in the shallow mantle at each side of the ridge axis and the material was then transported through these cells to the ridge axis. Alternatively, material from the continental crust has been trapped within the Kane fracture zone since the opening of the Atlantic Ocean basin through a series of transform migrations and ridge jumps (Bonatti and Crane, 1982, doi:10.1038/300343a0; Kepezhinskas and Dmitiev, 1992), with portions of this material subsequently migrating down the ridge axis.
description: Supplement to: Pilot, Joachim; Werner, Carl-Dietrich; Haubrich, Frank; Baumann, Nils (1998): Palaeozoic and Proterozoic zircons from the Mid-Atlantic Ridge. Nature, 393(6686), 676-679
DOI: 10.6084/m9.figshare.28743023.v1
title: Virus transport in density-dependent ASR

description: The data provided here for collecting model outputs and plotting figures in our paper.
DOI: 10.1594/pangaea.762492
title: (Table 1) Oxygen and carbon isotope compositions of altered carbonates from DSDP Hole 6-53 from the western Pacific Ocean

description: In the lower part of DSDP core 53.0, partly recrystallized carbonate sediments and well recrystallized limestone breccias of Oligo-Miocene age are associated with altered volcanic flows, lithified tuffs, and tuff breccias, suggesting that carbonate alteration was the result of thermal metamorphism. However, the oxygen isotope compositions of these carbonates (-3.4 to +0.6 per mil rel. PDB) are not compatible with recrystallization and isotope exchange with sea water at high temperatures. Evaluating the effects of the composition of the water which exchanged with the carbonates and of carbonate-water isotope exchange in closed systems yields the following approximate maximum temperature of recrystallization: limestone breccias, 100°C; calcite veins rimming breccia clasts, 30°C; and unconsolidated sediments overlying the breccias, 20°C. Therefore, the volcanics at site 53.0 must have been emplaced into the primary carbonate sediments at relatively low temperatures. Subsequent carbonate alteration was probably a consequence of chemical changes in ambient pore waters resulting from the submarine weathering of volcanic material.
description: Supplement to: Anderson, Thomas F (1973): Oxygen and carbon isotope compositions of altered carbonates from the western Pacific, Core 53.0, Deep Sea Drilling Project. Marine Geology, 15(3), 169-180
DOI: 10.1594/pangaea.815222
title: (Table 1) Organic geochemistry at DSDP Leg 71 Holes

description: Forty-three core samples from Sites 511 through 514 of DSDP Leg 71 were analyzed geochemically. The black shales at the bottom of Hole 511, in the basin province of the Falkland Plateau, contain an average of 1590 ppm extractable organic matter (EOM) and 120 ppm hydrocarbons. Whereas molecular type-carbon number distributions of mono- and polynuclear aromatic hydrocarbons and their sulphur and oxygen analogues in the black shale "aromatic hydrocarbon" fractions are very similar to those of many crude oils, other data - gas chromatography (GC) fingerprint, pyrolysis GC, visual kerogen analysis, H/C ratio - suggest the black shale section is thermally immature. Together, these observations imply that many of the hydrocarbons were deposited with the original sediments or are diagenetic products of other biological compounds. Pyrograms of the humic acid and kerogen fractions from the black shale interval are typical of geopolymers derived from marine algal material. It appears that these humic acids and kerogens are derived from the same lipid stock.
description: Supplement to: Copelin, E C; Larter, S R (1983): Chemical characterization of aromatic hydrocarbons, kerogen, and humic acids in Deep Sea Drilling Project Leg 71 Cores. In: Ludwig, WJ; Krasheninnikov, VA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 71, 1045-1049
DOI: 10.5281/zenodo.14280234
title: Supplemental Information:Iron isotope evidence for heightened primary productivity triggered by hydrothermally sourced nutrients during Oceanic Anoxic Event 2

description: The supplementary data used in the manuscript titled "Iron isotope evidence for heightened primary productivity triggered by hydrothermally sourced nutrients during Oceanic Anoxic Event 2", including newly measured bulk iron isotope and concentration values of Gongzha section, as well as coding scripts in MATLAB for modeling of osmium, carbon and iron isotopes cycling in the early stage of OAE2.
DOI: 10.5281/zenodo.14280235
title: Supplemental Information:Iron isotope evidence for heightened primary productivity triggered by hydrothermally sourced nutrients during Oceanic Anoxic Event 2

description: The supplementary data used in the manuscript titled "Iron isotope evidence for heightened primary productivity triggered by hydrothermally sourced nutrients during Oceanic Anoxic Event 2", including newly measured bulk iron isotope and concentration values of Gongzha section, as well as coding scripts in MATLAB for modeling of osmium, carbon and iron isotopes cycling in the early stage of OAE2.
DOI: 10.1594/pangaea.756084
title: (Table 1b) Chemical and isotopic composition of waters from the Yankicha Island and Kraternaya Bay at the thermal spring site II
DOI: 10.1594/pangaea.787188
title: (Table 2) Concentration and isotopic composition of helium in gases from mineral waters of the Taman Peninsula and Caucasus
DOI: 10.1594/pangaea.856775
title: (Table 3) Stable water isotopes of sediment cores YC12-HP-Mc and PG2100
DOI: 10.1594/pangaea.784670
title: (Table 5) Average chemical and isotopic compositions of waters from the caldera of the Haakon Mosby mud volcano
DOI: 10.1594/pangaea.860589
title: δ¹³C measurements on lipids of sediment core PS51/154-11
DOI: 10.1594/pangaea.753230
title: (Table 2) K-Ar age of basalts from the Indian Ocean floor
DOI: 10.1594/pangaea.774173
title: (Table T1) Sediment and pore water nitrogen and d15N concentrations of ODP Hole 202-1234A

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.910786
title: Planktic foraminifera stable carbon and oxygen isotope records of IODP Hole 353-U1443A
DOI: 10.1594/pangaea.773398
title: (Table T1) Sediment and pore water composition of ODP Hole 201-1230A
DOI: 10.1594/pangaea.823351
title: (Table 1) Petrography at DSDP Leg 55 Holes
DOI: 10.1594/pangaea.789006
title: (Table 1d) Principal petrographic characteristics and K-Ar isotope-geochronological data on samples from the Late Neopleistocene - Holocene activity phase of the Keli Volcanic Highland
DOI: 10.1594/pangaea.846289
title: (Fig. 3) Stable isotope record of Neogloboquadrina pachyderma sinistral in sediment core PS2644-5
DOI: 10.1594/pangaea.820816
title: (Table 1) Oxygen, sulfur, and carbon isotopic composition of pore water and of cores in DSDP Leg 59 Holes

description: Sediment depth is given in mbsf. Empty cells mean no data.
DOI: 10.1594/pangaea.902646
title: Carbon stable isotopes in a sediment core from Lake Otjikoto, Namibia
DOI: 10.1594/pangaea.788614
title: (Table 1) K-Ar age determinations for volcanic rocks of the Western Kamchatka-Koryak volcanogenic belt
DOI: 10.1594/pangaea.756560
title: Geochemical data for drilled powder samples from two fossil Porites corals from Integrated Ocean Drilling Program Expedition 310

description: Fossil corals are unique archives of past seasonal climate variability, providing vital information about seasonal climate phenomena such as ENSO and monsoons. However, submarine diagenetic processes can potentially obscure the original climate signals and lead to false interpretations. Here we demonstrate the potential of laser ablation ICP-MS to rapidly detect secondary aragonite precipitates in fossil Porites colonies recovered by Integrated Ocean Drilling Program (IODP) Expedition 310 from submerged deglacial reefs off Tahiti. High resolution (100 µm) measurements of coralline B/Ca, Mg/Ca, S/Ca, and U/Ca ratios are used to distinguish areas of pristine skeleton from those afflicted with secondary aragonite. Measurements of coralline Sr/Ca, U/Ca and oxygen isotope ratios, from areas identified as pristine, reveal that the seasonal range of sea surface temperature in the tropical south Pacific during the last deglaciation (14.7 and 11 ka) was similar to that of today.
description: The corals were sampled from the top (youngest) part to the bottom (oldest) part [DISTANCE]
description: Supplement to: Hathorne, Ed C; Felis, Thomas; James, Rachael H; Thomas, Alexander L (2011): Laser ablation ICP-MS screening of corals for diagenetically affected areas applied to Tahiti corals from the last deglaciation. Geochimica et Cosmochimica Acta, 75, 1490-1506
DOI: 10.1594/pangaea.823099
title: (Table 1) Carbon and isotopic composition of organic carbon in sediments from DSDP Leg 56 Holes

description: We have analyzed inorganic and organic carbons and determined the isotopic composition of both sedimentary organic carbon and inorganic carbon in carbonates contained in sediments recovered from Holes 434, 434A, 434B, 435, and 435A in the landward slope of Japan and from Hole 436 in the oceanic slope of the Japan Trench. Both inorganic and organic carbons were assayed at the P. P. Shirshov Institute of Oceanology, in the same sample, using the Knopp technique and measuring evolved CO2 gravimetrically. Each sample was analyzed twice in parallel. Measurements were of a ±0.05 per cent accuracy and a probability level of 0.95. Carbon isotopic analysis was carried out on a MI-1305 mass spectrometer at the I. M. Gubkin Institute of Petrochemical and Gas Industry and the results presented as dC13 values related to the PDB standard. The procedure for preparing samples for organic carbon isotopic analysis involved (1) drying damp sediments at 60°C; (2) treating samples, while heating, with 10 N HCl to remove carbonate carbon; and (3) evaporating surplus HCl at 60°C. The organic substance was turned to CO2 by oxidizing it in an oxygen atmosphere. To prepare samples for inorganic carbon isotopic analysis we decomposed the carbonates with orthophosphoric acid and refined the gas evolved. The dC13 measurements, including a full cycle of sample preparation, were of a ±0.5 per cent accuracy and a probability level of 0.95.
description: Sediment depth is given in mbsf. Empty cells = no data.
description: Supplement to: Romankevich, Evgeny A; Nesterova, Maria P; Shadsky, I P; Grinchenko, J I (1980): Carbon and Its isotopic composition in Pacific Ocean bottom sediments, Leg 56, Deep Sea Drilling Project. In: Scientific Party, Initial Reports of the Deep Sea Drilling Project, 56/57 (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 56-57, 1313-1317
DOI: 10.3886/icpsr09220.v2
title: National Health Interview Survey, 1978: Smoking Supplement
title: Version 2

description: The basic purpose of the Health Interview Survey (HIS) is to
obtain information about the amount and distribution of illness, its
effects in terms of disability and chronic impairments, and the kinds
of health services people receive. The 1978 Smoking Supplement provides variables from the core Person File (see HEALTH INTERVIEW SURVEY, 1978 [ICPSR 8044])including sex, age, race, marital status, veteran status, education, income, industry and occupation codes, and limits on activity. The variables unique to this supplement include information on smoking status of respondents including whether they never smoked, occasionally smoked, were former smokers, or were present smokers. Data are also supplied on number of cigarettes smoked,
age when started smoking, brands smoked, number of attempts to quit
smoking, and tar and nicotine levels of brands smoked.
description: These data contain multiple weight variables for each part. Users should refer to the User Guide for further information regarding the weights and their derivation. Additionally, users may need to weight the data prior to analysis.
description: A multistage probability sample was used in selecting housing units.
description: Datasets: 
DS1: National Health Interview Survey, 1978: Smoking Supplement
description: Civilian, noninstitutionalized population of the United
States and the District of Columbia from 1,924 geographically defined
Primary Sampling Units (PSUs).
description: face-to-face interviewThese data files contain weights, which must be used in any analysis.Per agreement with the National Center for Health Statistics (NCHS), ICPSR distributes the data files and text of the technical documentation for this collection as prepared by NCHS.The supplements to the Health Interview Surveys may be
used independently, since they incorporate the person file data for
this subset. The National Center for Health Statistics now refers to
these supplements as current health topics. The data contain ampersands
(&), dashes (-), and blank codes.
DOI: 10.1594/pangaea.835213
title: Foraminiferal records of Neogloboquadrina dutertrei from sediment core WIND28K
DOI: 10.1594/pangaea.871228
title: A new high-resolution pollen sequence at Lake Van, Turkey, during MIS 6-7

description: A new detailed pollen and oxygen isotope record of the penultimate interglacial-glacial cycle, corresponding to the Marine Isotope Stage (MIS) 7–6 (c. 242.5–131.2 ka before present), has been generated from the "Ahlat Ridge" (AR) sediment core at Lake Van, Turkey. The presented record displays the highest temporal resolution for this interval with a mean sampling interval of ~540 years.Integration of all available proxies shows three intervals of effective moisture, evidenced by the predominance of forested landscapes (oak-pine steppe forest), which can be correlated with MIS 7e, 7c, and 7a. The warmest stage in terms of highest temperate tree percentages is MIS 7c, while the amplitude of MIS 7e appears to be truncated by a shift to colder/drier climatic conditions. The detailed comparison between the penultimate interglacial complex (MIS 7) to the last interglacial (Eemian, MIS 5e) and the current interglacial (Holocene, MIS 1) provides a vivid illustration of possible differences of successive climatic cycles. Intervening periods of open steppe landscape correlate with MIS 7d and 7a, favouring local erosion and detrital sedimentation. The predominance of steppe elements during MIS 7d indicates very cold/dry climatic conditions. In contrast, the occurrence of more temperate tree percentages throughout MIS 7b points to relatively mild conditions, in agreement with atmospheric CO2 concentration and oxygen isotope records.Despite the general dominance of dry/cold desert-steppe vegetation during the penultimate glacial (MIS 6), this period can be divided into two parts: an early stage (c. 193–157 ka BP) with pronounced oscillations in tree percentages, and a later stage (c. 157–131 ka BP) with lower tree percentages and subdued oscillations. The occurring vegetation pattern is analogous to the MIS 3 to MIS 2 division during the last glacial in the same sedi–159 ka BP) as described in marine pollen records, which indicates cooler but relatively wetter climate conditions during the penultimate glacial.In comparison with long European pollen records, speleothem isotope records from the Near East, and global climate parameters (e.g., insolation, atmospheric CO2 content), the new high-resolution Lake Van record presents an improved insight into regional vegetation dynamics and climate variability in the eastern Mediterranean region.
description: Supplement to: Pickarski, Nadine; Litt, Thomas (2016): A new high-resolution pollen sequence at Lake Van, Turkey: Insights into penultimate interglacial-glacial climate change on vegetation history. Climate of the Past Discussions, 29 pp
DOI: 10.1594/pangaea.779744
title: Figure 5. Stable oxygen isotope ratios on Neogloboquadrina pachyderma of sediment core MD95-2029
DOI: 10.1594/pangaea.809828
title: (Table 1) Organic carbon, δ¹³C, CaCO3 and water in rock at DSDP Hole 76-534
DOI: 10.1594/pangaea.813421
title: (Table 1) Results of Rb-Sr measurements in Upper Vendian clayey rocks of the Russian Platform from the borehole Gavrilov_Yam_1 (samples from depths below 2400 m)
DOI: 10.1594/pangaea.869242
title: (Table S2) Stable isotope data (δ¹³C) of deep-dwelling planktic foraminifera Globorotaloides hexagonus from ODP Site 202-1240 (00°01' N, 82°27' W)
DOI: 10.1594/pangaea.785866
title: (Table A) Isotopic composition of mud-volcanic waters from the Taman Peninsula
DOI: 10.1594/pangaea.813422
title: (Table 2) Results of Rb-Sr measurements in Upper Vendian clayey rocks of the Russian Platform from the borehole Gavrilov_Yam_1 (samples from depths above 2400 m)
DOI: 10.1594/pangaea.785869
title: (Table B) Isotopic composition of mud-volcanic waters from Kakheti, Eastern Georgia
DOI: 10.1594/pangaea.764065
title: (Table 1) Physicochemical parameters and microbiological characteristics of the Kara Sea water column in September 2007
DOI: 10.1594/pangaea.821400
title: (Table 3) Oxygen isotopes in vein minerals at DSDP Hole 58-446A

description: Empty cells = no data.
DOI: 10.1594/pangaea.779745
title: Figure 5. Stable oxygen isotope ratios on Neogloboquadrina pachyderma of sediment core MD95-2033
DOI: 10.1594/pangaea.834412
title: (Table S1) Oxygen and silicon stable isotopes of diatom silica of sediment core SO202-27-6 during MIS 3

description: A new version of d18O measurement with an adjusted age model can be found here: doi:10.1594/PANGAEA.887504.
DOI: 10.1594/pangaea.807137
title: (Table 2) Carbon geochemistry and isotopes at DSDP Leg 81 Holes
DOI: 10.1594/pangaea.834320
title: (Table S4A) Oxygen and silicon stable isotopes of diatom silica of sediment core SO202-27-6
DOI: 10.1594/pangaea.841965
title: Tidal variations at buoy V12 (Jade Bay) from January to November 2010
DOI: 10.1594/pangaea.788029
title: (Table 4a) Chemical composition of metamorphic rocks from the upper unit of the Khavyven Highland
DOI: 10.1594/pangaea.820838
title: Stable isotopes measured on sediment core PS75/100-4TC
DOI: 10.1594/pangaea.833421
title: Stable isotopes measured on Cibicidoides spp. of sediment core PS75/059-2

description: The ages are based on the correlation to the LR04 benthic d18O stack. For ages based on correlation of the respective Fe content records to EDC dust contents on the AICC12 age scale, see Lamy et al., 2014, doi:10.1594/PANGAEA.826600.
DOI: 10.1594/pangaea.860737
title: Stable oxygen isotope record of Neogloboquadrina pachyderma (s) of sediment core PS75/085-1
DOI: 10.1594/pangaea.783716
title: (Table 1) Oxygen and carbon isotope compositions, 87Sr/86Sr ratio, and mineralogy of carbonate and carbonate-barite inclusions from sediments of the Deryugin Basin (Sea of Okhotsk)

description: Mineral composition of carbonate-barite inclusions is based on the XRD, SEM, and optical microscopy data.
DOI: 10.1594/pangaea.820837
title: Stable isotopes measured on sediment core PS75/100-4
DOI: 10.1594/pangaea.861972
title: Stable isotopes, radionuclides, and calculated sea surface temperature of sediment core ANSIC-03_342
DOI: 10.1594/pangaea.745902
title: (Table 4) Isotopic composition of sulfur and organic carbon in sulfide ores from hydrothermal fields at the axis of the East Pacific Rise near 9°50'N
DOI: 10.25318/3310056901-fra
title: Nombre d'entreprises canadiennes, sans employés, juin 2022

description: Nombre d'entreprises canadiennes, nombre d'emplacements sans employés, selon le Système de classification des industries de l'Amérique du Nord (SCIAN), Canada et provinces, juin 2022.
DOI: 10.15468/dl.rzqayw
title: Occurrence Download

description: A dataset containing 2071 species occurrences available in GBIF matching the query:
{
 "DatasetKey" : [
 "is 2004 Royal Haskoning Ltd Fal Estuary maerl and associated infauna core and grab survey"
 ]
}

 The dataset includes 2071 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000569-250214102907787/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.u6xb5v
title: Occurrence Download

description: A dataset listing the 1 species recorded in GBIF matching the query:
{
 "and" : [
 "Country is Canada",
 "TaxonKey is Euchirograpsus americanus A.Milne-Edwards, 1880"
 ]
}

 The dataset's 1 records were derived from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000567-250214102907787/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.15468/dl.k7776k
title: Occurrence Download

description: A dataset containing 2 species occurrences available in GBIF matching the query:
{
 "and" : [
 "BasisOfRecord is one of (Observation, Machine Observation, Human Observation, Specimen, Living Specimen)",
 "Continent is one of (South America, North America)",
 "HasCoordinate is true",
 "HasGeospatialIssue is false",
 "OccurrenceStatus is Present",
 "TaxonKey is Fragaria vesca f. alba (Duchesne) Staudt",
 "Year 1901-2025"
 ]
}

 The dataset includes 2 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000570-250214102907787/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.
DOI: 10.7303/syn63358724.7
title: Clinical Dataset
DOI: 10.15468/dl.mfmp4b
title: Occurrence Download

description: A dataset containing 1 species occurrences available in GBIF matching the query:
{
 "and" : [
 "Country is Canada",
 "TaxonKey is Euchirograpsus americanus A.Milne-Edwards, 1880"
 ]
}

 The dataset includes 1 records from 1 constituent datasets; see https://api.gbif.org/v1/occurrence/download/0000571-250214102907787/datasets/export for details.
 
Data from some individual datasets included in this download may be licensed under less restrictive terms.