cometadata/datacite-titles-descriptions-related-identifiers huggingface dataset:
DOI: 10.1594/pangaea.718891
title: Radiosonde measurements from station Bondville (2003-12)

description: Start location: Lincoln, IL; Distance from radiation site: 82 km; If launch time is exactly 00Z or 12Z, the actual launch time is likely unknown
DOI: 10.1594/pangaea.941654
title: Other measurements at 30 m from station Payerne (2021-01)
DOI: 10.1594/pangaea.671882
title: Basic measurements of radiation at station Regina (2003-07)
DOI: 10.1594/pangaea.773470
title: Headspace-gas measurements from IODP Hole 316-C0006E

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.773702
title: Core-section summary from IODP Hole 316-C0006F
DOI: 10.1594/pangaea.931360
title: Ultra-violet measurements from station Izaña (2021-03)
DOI: 10.1594/pangaea.773704
title: Electrical conductivity from IODP Hole 316-C0006F

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.707502
title: Meteorological synoptical observations from station Payerne (1993-01)
DOI: 10.1594/pangaea.941662
title: Ultra-violet measurements from station Payerne (2021-02)
DOI: 10.1594/pangaea.773874
title: Thermal conductivity of IODP Hole 316-C0007A

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.773792
title: Core-section summary from IODP Hole 316-C0007A
DOI: 10.1594/pangaea.941799
title: Other measurements at 30 m from station Payerne (2021-09)
DOI: 10.1594/pangaea.547885
title: Nutrients measured on water bottle samples at station Bm_1997-09-12_3, Bajo Molle, Chile
DOI: 10.1594/pangaea.671797
title: Basic measurements of radiation at station Regina (1996-05)
DOI: 10.1594/pangaea.931361
title: Radiosonde measurements from station Izaña (2021-03)

description: Start location: Guimar; Distance from radiation site: 5 km
DOI: 10.1594/pangaea.739439
title: Pollen profile LEDN86, Lake Lednica, Poland

description: Method: KOH, acetolysis (Faegri and Iversen, 1975). Mineral sapmles pretreated with HF.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.773855
title: Fossil occurrence of radiolarians from IODP Hole 316-C0007A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.907518
title: Experiment on epibacterial abundance on surface of Agarophyton

description: In order to assess the effect salinities and time points on bacterial cell density on surface of the alga, epibacterial cell density from T1 and T2 (n=5 for each salinity level and each time point) was determined via fluorescence microscopy of DAPI-stained bacterial cells. Epibacterial cell density samples from T0 were generated from 5 individuals prior to start of the treatment to obtain cell density values from T0. For methodological details, see Appendix S1 in supplementary information. Briefly, the bacteria attached to the surface of a defined quantity of Agarophyton were suspended in seawater via sonification and vortexing with sterile glass beads. The cells were then enriched on nitrocellulose filters, stained using standard techniques, and counted under epiﬂuorescence microscopy, and the results were standardized based on the sampled thallus area.
description: T0=timepoint in May 2015T1=timepoint in August 2015T2=timepoint in Oct 2015
description: Supplement to: Saha, Mahasweta; Künzel, Sven; Meichssner, Rafael; Neulinger, Sven C; Petersen, Finn Ole; Weinberger, Florian (2020): Salinity and Time Can Alter Epibacterial Communities of an Invasive Seaweed. Frontiers in Microbiology, 10
DOI: 10.1594/pangaea.941663
title: Radiosonde measurements from station Payerne (2021-02)
DOI: 10.1594/pangaea.670295
title: Basic and other measurements of radiation at Neumayer Station (2003-09)
DOI: 10.1594/pangaea.941666
title: Other measurements at 30 m from station Payerne (2021-02)
DOI: 10.1594/pangaea.848528
title: Particle characterization at CVAO during the 2008 Intensive III

description: Mass: Mettler-Toledo UMT2 after 48 h equilibration of the impactor foils at 20 °C and 50 % rel. humidity.IC: Parts of the impactor foils (about 30 %) were extracted by the identical method in 1.5 ml high purity water (&gt;18.1 ohm cm). Sample extracts were filtered through a 0.45 µm one-way syringe filter to remove insoluble materials prior to ion analysis. Ion analysis was performed for cations Na+, [NH4]+, K+, Mg2+, Ca2+ and anions Cl-, [NO2]-, [NO3]-, [SO4]2- and [C2O4]2-(KOH for anions and MSA for cations) and micromembrane suppression. using a standard ion-chromatography technique (ICS3000, DIONEX, USA) using automatic eluent generation For the anion separation a combination of AG18 and AS18 (2 mm) was applied while for the cation separation CG16 and CS16 (3 mm) were used. Chromatographic calibrations were carried out daily using a four point standard (Fluka, Switzerland).CE: Spectra Phoresis 1000 (TSP, USA), equipped with fused silica capillary (length: 70 cm, 63 cm to detector, ID: 75µm). For separation of dicarboxylic acids and methane sulfonic acic, the capillary was filled with a background electrolyte consisting of 10mmol l-1 p-aminobenzoic acid, 8 mmol l-1 diethylenetriamine, and 3.5 mmol l-1 aqueous sodium hydroxide (pH = 9.6). After hydrodynamic injection at 10.3 kPa for 34 s, a separation voltage of 30 kV was applied. Indirect detection was performed at 254 nm.OC/EC: modified VDI2465 Bl.2 using a C-mat 5500 at Tmax = 650 °C (OC: 8 min at 650 °C under high purity Nitrogen; EC: 8 min at 650 °C under high purity Oxygen). OM was calculated according to the paper of Turpin et al. 2000 (doi:10.1016/S1352-2310(99)00501-4) from OC using a factor of 2.TXRF: Bruker S2 Picofox on quartz wafers after 1.5 h cold plasma pyrolysis to eliminate the Nuclepore substrate.
DOI: 10.1594/pangaea.941673
title: Radiosonde measurements from station Payerne (2021-03)
DOI: 10.1594/pangaea.941674
title: Other measurements at 10 m from station Payerne (2021-03)
DOI: 10.1594/pangaea.774627
title: Xray-ct-scanner images from IODP Hole 316-C0006D

description: Geocode = [m CSF-A] Top Core depth (below sea floor).Measurements data just above (negative section depth) and below (depth exceed section length) a core section are utilized in the deconvolution (http://en.wikipedia.org/wiki/Deconvolution).
DOI: 10.1594/pangaea.941699
title: Ultra-violet measurements from station Payerne (2021-04)
DOI: 10.1594/pangaea.941826
title: Other measurements at 10 m from station Payerne (2021-11)
DOI: 10.1594/pangaea.733116
title: (Table 33) Chemical composition of magmatic rocks from DSDP Hole 49-410
DOI: 10.1594/pangaea.707592
title: Meteorological synoptical observations from station Payerne (2000-05)
DOI: 10.1594/pangaea.941828
title: Other measurements at 30 m from station Payerne (2021-11)
DOI: 10.1594/pangaea.750593
title: Meteorological observations during MAIDSTONE cruise from St. Johns to St. Johns started at 1779-05-15
DOI: 10.1594/pangaea.783604
title: Meteorological synoptical observations from Neumayer Station (2011-08)
DOI: 10.1594/pangaea.932191
title: Meteorological synoptical observations from station Tateno (2021-03)
DOI: 10.1594/pangaea.943024
title: At surface behaviour at absolute time of Weddell seal FIL2021_wed_a_f_01 from expedition FIL2021
DOI: 10.1594/pangaea.773878
title: Visual core description (VCD) from IODP Hole 316-C0007A

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.655060
title: Hydrochemistry measured on water bottle samples during Professor Siedlecki cruise PSied90/1
DOI: 10.1594/pangaea.929101
title: δ13C and δ18O isotopes of Globigerina bulloides from ODP Site 177-1090

description: Over the last deglaciation there were two transient intervals of pronounced atmospheric CO2 rise; Heinrich Stadial 1 (17.5-15 kyr) and the Younger Dryas (12.9-11.5 kyr). Leading hypotheses accounting for the increased accumulation of CO2 in the atmosphere at these times invoke deep ocean carbon being released from the Southern Ocean and an associated decline in the global efficiency of the biological carbon pump. From core ODP1090 we present new G. bulloidies carbon and oxygen isotope records. These stable isotopic analyses were performed on a Thermo Finnigan MAT253 coupled with a Kiel IV carbonate device at the University of Southampton.
DOI: 10.1594/pangaea.730448
title: (Table 81) Chemical composition of vein celadonite from basalts of the Nauru Basin, DSDP Hole 61-462

description: Analyses have been carried out by I. Romanenko in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences.
DOI: 10.1594/pangaea.929554
title: Soil temperature and relative humidity measurements in 5 cm soil depth at the Yungay hyperarid site in 2017
DOI: 10.1594/pangaea.930350
title: Basic measurements of radiation at station Billings (2019-04)
DOI: 10.1594/pangaea.760385
title: (Table 2) Composition of the main mass of picrite basalts from the Loihi Volcano
DOI: 10.1594/pangaea.484812
title: Color RGB values of multicorer GeoB7829-3, tube 3
DOI: 10.1594/pangaea.942995
title: Water temperature and salinity data from Weddell seal FIL2021_wed_a_f_01 from expedition FIL2021
DOI: 10.1594/pangaea.773890
title: Color data from IODP Hole 316-C0008B

description: Geocode = [m CSF-A] Top Core depth (below sea floor)
DOI: 10.1594/pangaea.610914
title: Underway carbon dioxide in the Indian Ocean of Marion-Dufresne cruise 35MF20070104

description: The resolution of the CO2 gas analyzer is 0.5 µatm with an uncertainty of &lt; 1 µatm based on average values for atmospheric xCO2 and 2 µatm for sea surface fCO2 (incl. SST correction)
DOI: 10.1594/pangaea.941701
title: Radiosonde measurements from station Payerne (2021-04)
DOI: 10.1594/pangaea.943026
title: At surface behaviour at absolute time of Weddell seal FIL2021_wed_a_f_02 from expedition FIL2021
DOI: 10.1594/pangaea.913645
title: Geochemical composition of tephra layers from deep sediment core GS16-204-22CC-A, Labrador Sea, North Atlantic

description: Electron-probe microanalysis (EPMA). These measurements were performed at the Tephrochronological Analytical Unit at the University of Edinburgh using a Cameca SX100 electron microprobe with five vertical wavelength dispersive spectrometers, providing oxide values (wt. %) for 10 major elements (see supplementary information).Beam size: 5Settings:cond1: Na, Al, Si, K†, Ca, Fe, Mgcond2: Mn, P†, Ti
DOI: 10.1594/pangaea.680513
title: Other measurements at 10 m from station Payerne (2006-06)
DOI: 10.1594/pangaea.746678
title: Chemical composition of basalt glasses from the Mid-Atlantic Ridge, Station 15S-18
DOI: 10.1594/pangaea.747289
title: Meteorological observations during ALBOROUGH cruise from Lisbon to Plymouth started at 1777-04-27
DOI: 10.1594/pangaea.815999
title: (Table 1) Trace metal/Ca ratios measured on Globigerinoides ruber shells of selected intervals at ODP Site 160-963

description: Sediment depth is given in mcd.
DOI: 10.1594/pangaea.783472
title: (Table A1) Rim-core-rim major element composition of microtektites from the microtektite/micrometeorite trapps from the Victoria Land Transantarctic Mountains

description: The traverse through microtektite 2-9.1 runs across a silica-rich inclusion (analyses No. 1-4). Spacing between individual analyses is 30 µm for microtektite 4.3, 7 µm for microtektite 2.1-9 and 20 µm for all other microtektites.
DOI: 10.1594/pangaea.931247
title: Stable carbon isotopes of sediment core MD-1
DOI: 10.1594/pangaea.942903
title: Meteorological synoptical observations from station Ishigakijima (2021-11)
DOI: 10.1594/pangaea.722159
title: Other measurements at 10 m from station Goodwin Creek (1995-12)

description: Version 2, 2009-06-24
DOI: 10.1594/pangaea.816951
title: (Table 1) Major-elements at DSDP Legs 68-70 Holes

description: Empty cells meand no data.
DOI: 10.1594/pangaea.711807
title: Basic measurements of radiation at station Carpentras (2007-01)
DOI: 10.1594/pangaea.835482
title: Hydrochemistry measured on water bottle samples during HEINCKE cruise HE203/1
DOI: 10.1594/pangaea.873660
title: Table 2 - CO2 accumulation parameters

description: An analytical solution to the equations describing the flow of a buoyant fluid released into a porous medium below a horizontal impermeable boundary is used to model the growth of CO2 accumulations beneath thin mudstone beds in the Utsira sand reservoir at Sleipner in the North Sea. Here supercritical CO2 has been injected at a rate of ab. 1 MT/yr since 1996 and imaged by time-lapse seismic data in 1999, 2001 and 2002. The CO2 rises as a narrow plume and is partially trapped by a number of thin mudstones before reaching the caprock to the reservoir. The radii of the individual layers of trapped CO2 increase as the square root of time since initiation as predicted by the modelling for constant input flux. However apparent negative initiation times for horizons low in the reservoir suggests that net input fluxes for these layers have decreased with time, most probably as the spreading layers have increased their leakage rates. Accumulation of CO2 in the layers higher in the reservoir was initiated up to 3 yr after injection started. Modelling of the thickness profiles across three of the higher layers suggests that their net input fluxes have increased with time. The observation that the central thicknesses of the deeper layers have remained approximately constant, or have slightly decreased since first imaged in 1999, is consistent with the model predictions that the central thickness is directly proportional to net input flux. However, estimates of the permeability of the reservoir from the rate of increase of the radii of the CO2 accumulations are an order of magnitude less than measured permeabilities on the reservoir sandstone. Permeabilities estimated from the modelling of layer thickness changes scatter in the same range. These discrepancies may arise from, 1) approximations in the model not being valid, 2) the measured permeabilities not being representative of the permeability for two-phase flow on the scale of the reservoir or, considered less likely, 3) that much less CO2 is being stored in the imaged CO2 accumulations than estimated from the seismic reflection profiles. The most probable cause of the discrepancy is that the relative permeability for the CO2 phase is significantly reduced at lower CO2 saturations.
description: Supplement to: Bickle, Mike; Chadwick, Andy; Huppert, Herbert E; Hallworth, Mark; Lyle, Sarah (2007): Modelling carbon dioxide accumulation at Sleipner: Implications for underground carbon storage. Earth and Planetary Science Letters, 255(1-2), 164-176
DOI: 10.1594/pangaea.874704
title: Bulk organic isotope geochemistry of sediment core BH03-3
DOI: 10.1594/pangaea.942904
title: Radiosonde measurements from station Ishigakijima (2021-11)
DOI: 10.1594/pangaea.858889
title: Table 6 Generalised properties of Utsira caprocks, based on analysis of cuttings (page 79)

description: Executive Summary: Carbon dioxide capture and storage (CCS) is one option for mitigating atmospheric emissions of carbon dioxide and thereby contributes in actions for stabilization of atmospheric greenhouse gas concentrations. The Bellona Foundation is striving to achieve wide implementation of carbon dioxide (CO2) capture and storage both in Norway and internationally. Bellona considers CCS as the only viable large scale option to close the gap between energy production and demand in an environmentally sound way, thereby ensuring that climate changes and acidification of the oceans due to increased CO2 concentrations in the atmosphere will be stabilised.ff
DOI: 10.1594/pangaea.721959
title: Other measurements at 10 m from station Goodwin Creek (2004-11)
DOI: 10.1594/pangaea.930972
title: Diatom percentage abundances and sea surface temperature reconstruction for core DA12-11/2-GC01 from the Iceland Basin

description: Here, we present datasets of diatom abundance and a diatom-based sea surface temperature reconstruction from the Iceland Basin. The 419.5 cm long marine sediment core DA12-11/2-GC01 was recovered in September 2012 by the Danish R/V Dana using a gravity corer. The core was taken from a location at the northern edge of the Gardar Drift and the eastern edge of the Björn Drift in the Iceland Basin (61.36.536 °N, 20.42.164 °W) at a water depth of 2120 m. Diatoms were analysed at 5 cm intervals over the upper 2 m of core, representing the period 6100-0 cal years BP, with chronological constraints provided by 6 radiocarbon dates. Diatoms were analysed using standard procedures, including the identification and counting of a minimum of 300 diatom per sample, which allowed calculation of the percentage abundances of different species. These abundances were converted into estimates of sea surface temperature using the weight averaging partial least squares transfer function approach.
DOI: 10.1594/pangaea.929508
title: Soil temperature and relative humidity measurements in 30 cm soil depth at the Yungay hyperarid site in 2015
DOI: 10.1594/pangaea.931248
title: Stable carbon isotopes of sediment core MD-2
DOI: 10.1594/pangaea.876976
title: Continuous sediment temperature observations at station BEFmate_S2low (2015-03)
DOI: 10.1594/pangaea.942910
title: Radiosonde measurements from station Ishigakijima (2022-01)
DOI: 10.1594/pangaea.909046
title: Correlation of sediment cores Burg17-C and Burg17-B
DOI: 10.1594/pangaea.943027
title: At surface behaviour at absolute time of Weddell seal FIL2021_wed_a_f_03 from expedition FIL2021
DOI: 10.1594/pangaea.668816
title: Basic measurements of radiation at station Carpentras (1997-02)
DOI: 10.1594/pangaea.730449
title: (Table 82) Chemical composition of basalts from the Nauru Basin at DSDP Site 61-462

description: Analyses have been carried out by S.P. Batalova and L.V. Shkodyuk (samples marked by *) in the Far East Geological Institute, Far East Scientific Center of the USSR Academy of Sciences.
DOI: 10.1594/pangaea.945100
title: Meteorological synoptical observations from station Abashiri (2022-03)
DOI: 10.1594/pangaea.682970
title: Continuous meteorological observations at Georg-von-Neumayer station (1990-08)

description: Geocode DATE/TIME has centered values.
DOI: 10.1594/pangaea.929514
title: Soil temperature and relative humidity measurements in 40 cm soil depth at the Yungay hyperarid site in 2015
DOI: 10.1594/pangaea.941955
title: Ultra-violet measurements from station Izaña (2022-02)
DOI: 10.1594/pangaea.835603
title: Temperature and photoperiod effects on sex determination in Leuresthes tenuis (fish)

description: In some gonochoristic species, sex is influenced not only by genotype at conception but also by the environment that offspring experience during early ontogeny (termed environmental sex determination or ESD). ESD is thought to be adaptive when seasonal variations in environmental conditions provide a sex-specific fitness advantage. In vertebrates, temperature is the most common determinant of sex, and seasonal variation in temperature serves as a temporal cue of environmental quality such as length of the growing season. Some environments, however, lack strong seasonal temperature fluctuations and other cues, particularly photoperiod, may provide a more reliable indicator of the environment offspring enter. We tested this hypothesis by rearing the offspring of the California grunion (Leuresthes tenuis, Ayres), which experiences low seasonal temperature variation in nature, under common garden conditions at three temperature and two photoperiod treatments. Our experiments revealed that both temperature and photoperiod significantly affected sex ratios in L. tenuis. More females were produced at cooler temperatures and longer day lengths, which is consistent with female biased sex ratios early in the breeding season, and likely adaptive through increased female size and fecundity. To our knowledge, this is the first documented case of photoperiod-dependent sex determination in a gonochoristic vertebrate.
description: Supplement to: Brown, Elizabeth E; Baumann, Hannes; Conover, David O (2014): Temperature and photoperiod effects on sex determination in a fish. Journal of Experimental Marine Biology and Ecology, 461, 39-43
DOI: 10.1594/pangaea.916308
title: 1-Hz PPP displacements at GEONET station 0101 during the 2011 Tohoku Mw9.0 earthquake
DOI: 10.1594/pangaea.843729
title: Experiment on effects of elevated pCO2 on bivalve dominated communities: Bacterial counts
DOI: 10.1594/pangaea.898001
title: Mercury intrusion porosimetry throat size distributions of specimens from the MEL-5 borehole core samples of Lipnice granite
DOI: 10.1594/pangaea.929557
title: Soil temperature and relative humidity measurements in 20 cm soil depth at the Yungay hyperarid site in 2017
DOI: 10.1594/pangaea.499812
title: Morphometric measures of individuals of Aulacomya atra in 1996, Independencia Bay, Peru
DOI: 10.1594/pangaea.665552
title: Oceanography at CTD/bottle station IFREMER_2392
DOI: 10.1594/pangaea.942996
title: Water temperature and salinity data from Weddell seal FIL2021_wed_a_f_02 from expedition FIL2021
DOI: 10.1594/pangaea.949675
title: Meteorological synoptical observations from station Tamanrasset (2022-09)
DOI: 10.1594/pangaea.862313
title: GPS-derived precipitable water vapor content calculated for station LAMA
DOI: 10.1594/pangaea.931249
title: Stable carbon isotopes of sediment core UD-4
DOI: 10.1594/pangaea.718366
title: Other measurements at 10 m from station Boulder, SURFRAD (1997-09)

description: Version 2, 2009-06-12
DOI: 10.1594/pangaea.749211
title: Meteorological observations during EMERALD cruise from New York to Uk started at 1783-08-05
DOI: 10.1594/pangaea.751363
title: Meteorological observations during Princess Augusta cruise from St. Helena to Falmouth started at 1762-05-18
DOI: 10.1594/pangaea.820009
title: (Table 3) Major elements of bulk samples at DSDP Holes 60-460 to 60-461

description: Empty cells = not analyzed.
DOI: 10.1594/pangaea.776414
title: (Fig. 4) Sedimentology of sediment core PG1984
DOI: 10.1594/pangaea.930429
title: Bioengineering experiment on Schiermonnikoog 2015: experimental effects on diatom composition and biovolume

description: In 2015 the Marine Ecology lab. (Eriksson Lab. at the Groningen Institute for Evolutionary Life Sciences [GELIFES], University of Groningen, The Netherlands); tested the effect of different intertidal bioengineering bivalve habitats on the sediment community. We did this by adding different small scale (0.5 by 0.5 m) bivalve assemblages to the intertidal; the treatments included blue mussel reefs, cockle beds, dead shell assemblages, different types of fencing a to protect the bivalves from bird and crab predation; and fencing controls to test for fence effects. We measured effects on sediment conditions (OM, cohesion, erosion), diatom community composition and development (species composition based on cell counts and biovolume, chlorophyll a concentrations), and infauna abundance. The field experiment in the intertidal ran from 30 April to 10 June 2015 and complementary field samples were collected around a natural blue mussel bed on the same tidal flat on 7 October 2015 (N 53.489, E 6.230 degrees).
description: Type of experiment: Biomanipulation; blue mussels were added to a tidal flat to test the effect of reefs on the diatom community. The experiment compared effects of adding mussels with not adding mussels to a bare sediment tidal flat. The experiment included two fence treatments (predation protection from birds [rope fence] and birds + crabs [plastic fence]), that were manipulated in a factorial design with the mussel additions. The experiment also included an unmanipulated control (no mussel additions; no fence around the plots) to be able to test for procedural fence effects. Start of experiment: 30 April 2015 End of experiment: 10 June 2015 (this is the time we took the samples)---Unmanipulated Control: C Bare flat + Rope fence: CB Bare flat + Plastic fence: FMussel additions + Rope fence: MMussel additions + Plastic fence: MF
DOI: 10.1594/pangaea.704822
title: Basic measurements of radiation at station Carpentras (2003-10)