cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.811050
title: (Table 1) Geochemical and geothermometry data from fibrous calcite vein fills in the Dabashan Fold Belt, China

description: Fibrous calcite veins with organic inclusions have been widely considered as indicators of oil and gas generation and migration under overpressure. Abundant fibrous calcite veins containing organic-bearing inclusions occur in faulted Lower Paleozoic through Triassic hydrocarbon source rocks in the Dabashan Foreland Belt (DBF). d13CPDB and d18OPDB values of the fibrous calcite range from - 4.8 to -1.9 to per mil and - 12.8 to - 8.4 per mil respectively, which is lighter than that of associated carbonate host rocks ranging from - 1.7 to + 3.1 per mil and - 8.7 to - 4.5 per mil. A linear relationship between d13CPDB and d18OPDB indicates that the calcite veins were precipitated from a mixture of basinal and surface fluids. The fibrous calcite contains a variety of inclusions, such as solid bitumen, methane bearing all-liquid inclusions, and vapor-liquid aqueous inclusions. Homogenization temperatures of aqueous inclusions range from 140 to 196° with an average of 179°. Salinities of aqueous inclusions average 9.7 wt% NaCl. Independent temperatures from bitumen reflectance and inclusion phase relationships of aqueous and methane inclusions were used to determine fluid pressures. Results indicate high pressures, elevated above typical lithostatic confining pressure, from 150 to 200 MPa. The elevated salinity and high temperature and pressure conditions of the fibrous calcite veins argue against an origin solely from burial overpressure resulting from clay transformation and dehydration reactions. Instead fluid inclusion P-T data and geochemistry results and regional geology indicate abnormally high pressures during fluid migration. These findings indicate that tectonic stress generated fracture and fault fluid pathways and caused migration of organic bearing fluids from the DBF during the Yanshan orogeny.
description: Supplement to: Li, Rongxi; Dong, Shuwen; Lehrmann, Daniel; Duan, Lizhi (2013): Tectonically driven organic fluid migration in the Dabashan Foreland Belt: evidenced by geochemistry and geothermometry of vein-filling fibrous calcite with organic inclusions. Journal of Asian Earth Sciences, 75, 202-212
DOI: 10.1594/pangaea.762480
title: (Table 1) Temperature and salinity of studied water samples from the Sea of Japan
DOI: 10.1594/pangaea.900812
title: Meteorological synoptical observations from Neumayer Station (2018-06)
DOI: 10.1594/pangaea.756112
title: Physical oceanography during Professor Vodyanitskiy cruise PV8
DOI: 10.1594/pangaea.931084
title: Ozone measurements from station Lindenberg (2018-11)
DOI: 10.1594/pangaea.842675
title: X-ray fluorescence on sediment core PG2070-1 (raw data from XRF-core scanner)

description: raw XRF, may contain contaminations
DOI: 10.1594/pangaea.746623
title: Trace and rare earth element contents in altered basalts from the Mid-Atlantic Ridge near 15°20'N
DOI: 10.1594/pangaea.842680
title: X-ray fluorescence on sediment core PG2075-1 (raw data from XRF-core scanner)

description: raw XRF, may contain contaminations
DOI: 10.1594/pangaea.940088
title: Expanded measurements from station Ny-Ålesund (2021-12)

description: 99999: No clouds detected
DOI: 10.1594/pangaea.728687
title: (Table 1) Distribution of Oligocene-Pleistocene calcareous nannofossils in ODP Hole 120-747A

description: Species abundances: V = very abundant (&gt;10 specimens per field of view), A = abundant (1-10 specimens per field of view), C = common (1 specimen per 2-10 fields of view), F = few (1 specimen per 11-50 fields of view), R = rare (1 specimen per 51-200 fields of view), r = rare reworked specimens, - = absent
DOI: 10.1594/pangaea.875833
title: Meteorological synoptical observations from station Lindenberg (2011-06)
DOI: 10.1594/pangaea.746514
title: Trace and rare earth element contents in dolerites from the Mid-Atlantic Ridge near 15°20'N
DOI: 10.1594/pangaea.939958
title: Radiosonde measurements from station Tateno (2021-10)
DOI: 10.1594/pangaea.876886
title: Continuous sediment temperature observations at station BEFmate_I3low (2015-03)
DOI: 10.1594/pangaea.930242
title: Long-term Globorotalia menardii (300-355 μm) stable isotopic compositions from IODP Site 359-U1467
DOI: 10.1594/pangaea.931178
title: Color reflectance from the Frankenbach loess-paleosol sequence in the Heilbronn Basin, southwestern Germany
DOI: 10.1594/pangaea.930244
title: Raw foraminiferal IODP Site 359-U1467 isotopic data for samples from the modern-day (mudline samples) and maxima/minima of MIS2, MIS11c and MIS12
DOI: 10.1594/pangaea.655125
title: Hydrochemistry measured on water bottle samples during SVANIC cruise Svanic90/2
DOI: 10.1594/pangaea.931184
title: Geochemical anaylsis from the Talheim loess-paleosol sequence in the Heilbronn Basin, southwestern Germany
DOI: 10.1594/pangaea.902123
title: Ozone measurements from station Tamanrasset (2019-04)
DOI: 10.1594/pangaea.931187
title: Rock magnetic data of the Frankenbach loess-paleosol sequence in the Heilbronn Basin, southwestern Germany
DOI: 10.1594/pangaea.930246
title: Raw foraminiferal IODP Site 359-U1467 Mg/Ca data for samples from the modern-day (mudline samples) and maxima/minima of MIS2, MIS11c and MIS12
DOI: 10.1594/pangaea.465171
title: Monthly density of benthic invertebrate postlarvae on nylon collectors in independencia Bay, 1997, Peru
DOI: 10.1594/pangaea.940178
title: Basic measurements of radiation at station Cener (2021-11)
DOI: 10.1594/pangaea.847334
title: Abundance and biomass of gelatinous plankton in the Black Sea in July 1992
DOI: 10.1594/pangaea.940179
title: Basic measurements of radiation at station Cener (2021-12)
DOI: 10.1594/pangaea.511188
title: Radiosonde at Georg-Forster station on 1989-09-25 12:00h

description: Height of tropopause 12389 m, total ozone 265.3 DU
DOI: 10.1594/pangaea.941635
title: Ozone measurements from station Payerne (2021-08)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.6084/m9.figshare.25568571.v2
title: An entity alignment approach coupling NGBoost and SHAP for Constructing Spatio-temporal Evolution Knowledge Graph from Historical Atlases

description: This is the data and codes that support the findings of the IJGIS paper "An entity alignment approach coupling NGBoost and SHAP for Constructing Spatio-temporal Evolution Knowledge Graph from Historical Atlases".
DOI: 10.1594/pangaea.750248
title: Meteorological observations during La Pintade cruise from Philadelphia to Baltimore started at 1783-09-05
DOI: 10.1594/pangaea.751753
title: Meteorological observations during RESOURCE cruise from Jamaica to Woolwich started at 1797-06-30
DOI: 10.1594/pangaea.941299
title: Basic measurements of radiation at station Palaiseau (2020-09)
DOI: 10.1594/pangaea.511172
title: Radiosonde at Georg-Forster station on 1989-03-22 12:00h

description: Height of tropopause 8917 m
DOI: 10.1594/pangaea.672765
title: Basic and other measurements of radiation at station South Pole (1995-04)
DOI: 10.1594/pangaea.773392
title: Thermal conductivity of IODP Hole 316-C0006D

description: Geocode = [m CSF-A] Top Core depth (below sea floor). Standard VLQ laboratory probe, source length is 70 mm and source diameter 2 mm. Measuring range 0.1 - 10 Wm-1K-1.
DOI: 10.1594/pangaea.941633
title: Ozone measurements from station Payerne (2021-06)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.930461
title: Obergurgl, AT, moraine1971, Micro- and Bio-climate time series in 1996
DOI: 10.1594/pangaea.941022
title: Ultra-violet measurements from station Izaña (2022-01)
DOI: 10.1594/pangaea.941634
title: Ozone measurements from station Payerne (2021-07)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.511262
title: Radiosonde at Georg-Forster station on 1992-01-17 00:00h

description: Height of tropopause 8489 m
DOI: 10.1594/pangaea.941638
title: Ozone measurements from station Payerne (2021-11)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.706581
title: Occurrence of microtextures recorded from quartz sand grains of ODP Hole 178-1101A (Table 1)

description: Sediment drifts on the continental rise are located proximal to the western side of the Antarctic Peninsula and recorded changes in glacial volume and thermal regime over the last ca. 15 m.y. At Ocean Drilling Program (ODP) Site 1101 (Leg 178), which recovered sediments back to 3.1 Ma, glacial-interglacial cyclicity was identified based on the biogenic component and sedimentary structures observed in X-radiographs, magnetic susceptibility and lithofacies descriptions. Glacial intervals are dominated by fine-grained laminated mud and interglacial units consist of bioturbated muds enriched in biogenic components. From 2.2 to 0.76 Ma, planktonic foraminifera and calcareous nannofossils dominate in the interglacials suggesting a shift of the Antarctic Polar Front (APF) to the south near the drifts. Prior to 2.2 Ma, cyclicity cannot be identified and diatoms dominate the biogenic component and high percent opal suggests warmer conditions south of the APF and reduced sea ice over the drifts. Analyses of the coarse-grained terrigenous fraction (pebbles and coarse sand) from Sites 1096 and 1101 record glaciers at sea-level releasing iceberg-rafted debris (IRD) throughout the last 3.1 m.y. Analyses of quartz sand grains in IRD with the scanning electron microscope (SEM) show an abrupt change in the frequency of occurrence of microtextures at ~1.35 Ma. During the Late Pliocene to Early Pleistocene, the population of quartz grains included completely weathered grains and a low frequency of crushing and abrasion, suggesting that glaciers were small and did not inundate the topography. Debris shed from mountain peaks was transported supraglacially or englacially allowing weathered grains to pass through the glacier unmodified. During glacial periods from 1.35-0.76 Ma, glaciers expanded in size. The IRD flux was very high and dropstones have diverse lithologies. Conditions resembling those at the Last Glacial Maximum (LGM) have been episodically present on the Antarctic Peninsula since ~0.76 Ma. Quartz sand grains show high relief, fracture and abrasion common under thick ice and the IRD flux is low with a more restricted range of dropstone lithologies.
description: The composite depth scales and age models of Barker (2002, doi:10.2973/odp.proc.sr.178.219.2001) were used to develop a chronology. The age of each sample collected from Sites 1101 was computed by linear interpolation between magnetostratigraphic datums from Acton et al. (2002, doi:10.2973/odp.proc.sr.178.235.2002).
description: Supplement to: Cowan, Ellen A; Hillenbrand, Claus-Dieter; Hassler, Lauren E; Ake, Matthew T (2008): Coarse-grained terrigenous sediment deposition on continental rise drifts: A record of Plio-Pleistocene glaciation on the Antarctic Peninsula. Palaeogeography, Palaeoclimatology, Palaeoecology, 265(3-4), 275-291
DOI: 10.1594/pangaea.750445
title: Meteorological observations during LILLY cruise from Halifax to St. Georges Bermuda started at 1799-12-23
DOI: 10.1594/pangaea.941639
title: Ozone measurements from station Payerne (2021-12)

description: Location: Arosa, Switzerland; Distance from radiation site: 200 km
DOI: 10.1594/pangaea.930464
title: Obergurgl, AT, moraine1971, Micro- and Bio-climate time series in 1997
DOI: 10.1594/pangaea.921510
title: Total dissolved solids and major ions in modern marine sediments on the Belyy Island
DOI: 10.1594/pangaea.930465
title: Obergurgl, AT, moraine1971, Micro- and Bio-climate time series in 1998
DOI: 10.1594/pangaea.547856
title: Nutrients measured on water bottle samples at station Bm_1997-09-04_1, Bajo Molle, Chile
DOI: 10.1594/pangaea.677109
title: Ozone measurements from station Boulder (1996-07)

description: Location: Boulder, Colorado, USA; Distance from radiation site: 16 km
DOI: 10.1594/pangaea.811424
title: (Table 1) Major and trace elements of basalts at DSDP Hole 72-516F

description: The geochemistry of basalts recovered during Leg 72 is described with emphasis on trace elements. Only Hole 516F penetrated basement; the basalts recovered are plagioclase-phyric and olivine-phyric and pervasively altered. Chemically, the basalts from Hole 516F are rather uniform in composition. However, four distinct geochemical units can be recognized, although the chemistry of two of the units appears to be controlled by chemical mobility associated with alteration. The two less-altered units cannot be related by fractional crystallization processes. Hole 516F basalts have a trace element chemistry characteristic of T-type mid-ocean ridge basalt; rare-earth element patterns (as indicated by Ce/Y ratios) are mildly fractionated flight rare-earth element enriched), and a number of incompatible element ratios are close to chondritic.
description: Supplement to: Weaver, Barry L; Marsh, Nicholas G; Tarney, J (1983): Trace element geochemistry of basaltic rocks recovered at Site 516, Rio Grande Rise, Deep Sea Drilling Project Leg 72. In: Barker, PF; Carlson, RL; Johnson, DA; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 72, 451-456
DOI: 10.1594/pangaea.921521
title: Cryohydrochemical characteristics of ice on Belyy Island and at other cryospheric and hydrospheric objects
DOI: 10.1594/pangaea.897204
title: Meteorological synoptical observations from station Tamanrasset (2018-12)
DOI: 10.1594/pangaea.807842
title: Sulphur hexafluoride (SF6) measured on water bottle samples during TANGAROA cruise SOIREE
DOI: 10.1594/pangaea.749412
title: Meteorological observations during GIBRALTAR cruise from Boston to Antigua started at 1771-02-21
DOI: 10.1594/pangaea.916799
title: 1-Hz PPP displacements at GEONET station 0610 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.750849
title: Meteorological observations during Na sa del Rosario cruise from Veracruz to Cuba started at 1794-05-22
DOI: 10.1594/pangaea.707623
title: Meteorological synoptical observations from station Payerne (2002-04)
DOI: 10.1594/pangaea.923973
title: Seawater carbonate chemistry and the response to cadmium of stress-related genes in Mytilus galloprovincialis

description: Anthropogenic inputs of carbon dioxide in the atmosphere are driving ocean warming and acidification. The potential threat represented by these changes for marine species could be amplified in coastal areas, characterized by higher levels of pollutants. In addition, temperate organisms may exhibit a different seasonal tolerance to stressors influenced by fluctuations of environmental and physiological factors. In this study, Mediterranean mussels Mytilus galloprovincialis collected both in summer and winter were exposed to combinations of two temperatures (SST, seasonal surface temperature and SST+5 °C) and two levels of pH (8.20 and 7.40) in clean or cadmium contaminated seawater (20 μg/L Cd). mRNA levels of genes related to metal-induced stress response were investigated, including metallothionein mt-20, heat-shock protein hsp70, superoxide dismutase Cu/Zn-sod, catalase cat, glutathione peroxidase gpx1 and glutathione S-transferase gst-pi. To further elucidate if tissues with different physiological roles could exhibit different responsiveness, such analyses were carried out in digestive gland and in gills of exposed mussels. mt-20 mRNA increase after Cd-exposure was higher in the digestive gland than in the gills, with few modulations by temperature or pH only in the latter. Acidification, alone or in combination with other stressors, increased hsp70 mRNA, with seasonal- and tissue-specificities (higher in summer and in digestive gland). Among antioxidants, gpx1 mRNA was affected by Cd in both tissues and seasons, with further modulations due to pH and temperature variation tissue- and season-specific; in winter the combination of Cd, warming and acidification affected Cu/Zn-sod both in digestive gland and gills and cat only in gills, while weak seasonal variations were observed for gst-pi transcripts only in digestive gland. The overall results highlighted the importance of considering seasonality and responsiveness of different tissues to predict the effects of sudden changes in environmental parameters on responsiveness to and toxicity of chemicals in marine coastal organisms.
description: In order to allow full comparability with other ocean acidification data sets, the R package seacarb (Gattuso et al, 2019) was used to compute a complete and consistent set of carbonate system variables, as described by Nisumaa et al. (2010). In this dataset the original values were archived in addition with the recalculated parameters (see related PI). The date of carbonate chemistry calculation by seacarb is 2020-10-14.
DOI: 10.1594/pangaea.921610
title: δ¹⁸O, δ²H, and dexc in the samples of massive ice of the left bank of the Erkutayaha River (southern Yamal) in July 2010

description: Variations in δ¹⁸O, δ²H, and dexc in the samples of massive ice sampled on the left bank of the Erkutayaha River (southern part of Yamal) in July 2010 (point 10-YuV-Yerk).The isotopic composition of ice was determined at the Geographical Faculty of Moscow State University in the Laboratory of Stable Isotopes of the Department of Landscape Geochemistry and Soil Geography (Prof. Yu. Vasil'chuk, Dr. N. Budantseva, Dr. Ju. Chizhova) using the Delta V mass spectrometer with the GasBench standard option. During the measurements of δ¹⁸О, the analyzed samples were stabilized in CO2 for 24 hours; stabilization for the δ²H measurements was performed for 40 min in the presence of a platinum stabilizer. The International Standard of Mean Ocean Water (SMOW V), the MAGATE International laboratory standards, and the standards of the Isotope Laboratory of the Austrian Institute of Technology were used to calibrate the measurements.
DOI: 10.1594/pangaea.941794
title: Other measurements at 30 m from station Payerne (2021-08)
DOI: 10.1594/pangaea.843810
title: The effect of repeated exposure to parasite genotypes of the eyefluke Diplostomum pseudospathaceum on infection rate and immunization in three-spined sticklebacks: Mass infection
DOI: 10.1594/pangaea.739841
title: Pollen profile SPISBELA, Spisska Bela, Slovakia

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.941782
title: Ultra-violet measurements from station Payerne (2021-07)
DOI: 10.1594/pangaea.941791
title: Ultra-violet measurements from station Payerne (2021-08)
DOI: 10.1594/pangaea.740177
title: Age determination of sediment core AVRIG1, Avrig, Romania

description: This dataset was archived on 2010-05-11 from the EPD database (http://www.europeanpollendatabase.net).
DOI: 10.1594/pangaea.931355
title: Radiosonde measurements from station Izaña (2021-04)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.669993
title: Basic measurements of radiation at station Kwajalein (2003-12)
DOI: 10.1594/pangaea.718003
title: Ultra-violet measurements from station Boulder, SURFRAD (2006-07)

description: UV-b values were originally given in mW/m² and then erroneously imported in W/m² using the same numbers. The numbers have been corrected (divided by 1000) on 2017-02-09.
DOI: 10.1594/pangaea.823554
title: (Table 2) Geochemistry of glasses at DSDP Leg 54 Holes

description: The compositions of 45 natural basalt glasses from nine dredge stations and six Deep Sea Drilling Project Leg 54 sites near 9°N on the East Pacific Rise have been determined by electron microprobe. These comprise 19 distinct chemical groups. Seventeen of these fall in the range of the eastern Pacific tholeiite suite, which is characterized by marked enrichment in FeO*, TiO2, K2O, and P2O5 as CaO, MgO, and Al2O3 all decrease. Based on trace elements, an estimated 50-75 per cent fractionation of plagioclase, clinopyroxene, and olivine is required to produce ferrobasalts from parental olivine tholeiites. Additional chemical variations occur which require source heterogeneities, differences in the degree of melting, different courses of shallow fractionation, or magma mixing to explain. Glass compositions from within the Siqueiros fracture zone are mostly less fractionated than those from the flanks of the Rise, and show chemical differences which require variations in the depth of melting or highpressure fractionation to explain. Some of them could not be parental to East Pacific Rise flank ferrobasalts. Two remaining glass groups, from dredge hauls atop a ridge and a seamount, respectively, have distinctly higher K2O, P2O5, and TiO2 as well as lower CaO/Al2O3 and SiO2 at corresponding values of MgO than the tholeiite suite. These abundances, and whole-rock Y/Zr, Ce/Y, Nb/Zr, and isotopic abundances indicate that these basalts had a deeper, less depleted mantle source than the Rise tholeiite suite. Trace element abundances preclude the "ridge" basalt type from being a hybrid between the "seamount" basalt type and any East Pacific Rise tholeiite so far analyzed. The East Pacific Rise glasses from 9°N compare very closely to glasses dredged and drilled elsewhere on the East Pacific Rise. However, glass compositions from Site 424 on the Galapagos Rift drilled during Leg 54, as well as glasses and basalts dredged from the Galapagos and Costa Rica rifts, indicate that a greater degree of melting prevailed along much of the Galapagos Spreading Center than anywhere along the East Pacific Rise.
description: Supplement to: Natland, James H; Melson, William G (1980): Compositions of basaltic glasses from the East Pacific Rise and Siqueiros Fracture Zone, near 9°N. In: Rosendahl, BR; Hekinian, R; et al. (eds.), Initial Reports of the Deep Sea Drilling Project (U.S. Govt. Printing Office), 54, 705-723
DOI: 10.1594/pangaea.941649
title: Ultra-violet measurements from station Payerne (2021-01)
DOI: 10.1594/pangaea.511176
title: Radiosonde at Georg-Forster station on 1989-08-01 12:00h

description: Height of tropopause 9128 m, total ozone 209.5 DU
DOI: 10.1594/pangaea.670275
title: Basic and other measurements of radiation at Neumayer Station (2001-10)
DOI: 10.1594/pangaea.807907
title: Particulate silica measured on water bottle samples during TANGAROA cruise SOIREE
DOI: 10.1594/pangaea.843813
title: The effect of repeated exposure to parasite genotypes of the eyefluke Diplostomum pseudospathaceum on infection rate and immunization in three-spined sticklebacks: RNA
DOI: 10.1594/pangaea.739608
title: Pollen profile NUSS4, Nussbaumer Seen, Switzerland

description: The EPD (http://www.europeanpollendatabase.net) accepted species name is given in the parameter comment. This dataset was archived on 2010-05-11 from the EPD database.
DOI: 10.1594/pangaea.848480
title: Zooplankton biomass from METEOR cruise M87/1 in April 2012

description: Zooplankton samples were taken in five depth strata using a Multinet type Midi, with 50 µm nets. The samples were taken during the second leg only, three times at station 1, two times at station 2 and once at station 3. Zooplankton were identified to species / genus and life-stage, and at least 300 individuals were counted per sample. 10 individuals of each stage / species were measured and the numbers of eggs counted.
DOI: 10.1594/pangaea.860457
title: Age model of sediment core MD76-135
DOI: 10.1594/pangaea.898902
title: Meteorological synoptical observations from Neumayer Station (2008-05)

description: Version 2, 2019-03-01 with some minor corrections to the codes.
DOI: 10.1594/pangaea.671341
title: Basic measurements of radiation at station Sede Boqer (2004-05)
DOI: 10.1594/pangaea.773771
title: Structure description (VCD) from IODP Hole 316-C0006F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.772947
title: Headspace-gas measurements from IODP Hole 315-C0002D

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.833311
title: Continuous meteorological observations at Neumayer station (2013-07)